水洞沟遗址的环境与地层

人类学学报 ›› 1988, Vol. 7 ›› Issue (03): 263-269.

水洞沟遗址的环境与地层

周昆叔,胡继兰

出版日期:1988-09-15 发布日期:1988-09-15

Environment and statigraphy at Shuidonggou Site

Zhou Kunshu, Hu Jilan

Online:1988-09-15 Published:1988-09-15

摘要/Abstract

摘要： 水洞沟第四纪地层可与萨拉乌苏河组上段对比。水洞沟遗址包含有新石器和旧石器晚期文化,其旧石器晚期文化发生在距今20,000多年至10,000多年间的黄土状粉砂土中,即发生在末次冰期主冰期的干冷环境下,比发育在距今约35,000—50,000年间的萨拉乌苏河旧石器文化为晚。

关键词: 水洞沟;孢粉分析;环境;地层

Abstract: The Shuidonggou site is 30 km northeast to Lingwu county in the Ningxia Hui Autonomous Region. Neolithic and Late Paleolithic remains were found at this site.
The results of field investigation, chronological research and sporo- pollen analysis show that the Quaternary of Shuidouggou could be correlated with the upper Salawusu river formation. The Late Paleolithic culture is dated to 20-10 thousand years BP. and under dry and cold climate of Pleniglacial of Last glacial.

Key words: Shuidonggou; Sporo-pollen analysis; Environment; Stratigraphy

周昆叔,胡继兰. 水洞沟遗址的环境与地层[J]. 人类学学报, 1988, 7(03): 263-269.

Zhou Kunshu, Hu Jilan. Environment and statigraphy at Shuidonggou Site[J]. Acta Anthropologica Sinica, 1988, 7(03): 263-269.